Kinematic models of a dry convective boundary layer compared with dual-Doppler radar observations of wind fields
- 1 June 1976
- journal article
- Published by Springer Nature in Boundary-Layer Meteorology
- Vol. 10 (3), 311-330
- https://doi.org/10.1007/bf00919392
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Observations of boundary-layer convection cells measured by dual-Doppler radar and echosonde, and by microbarograph arrayBoundary-Layer Meteorology, 1976
- Kinematic Structure and Flux Quantities in a Convective Storm from Dual-Doppler Radar ObservationsJournal of the Atmospheric Sciences, 1976
- Internal airflow of a convective storm from dual-Doppler radar measurementsPure and Applied Geophysics, 1975
- The Influence of a Capping Inversion on the Dynamic and. Convective Instability of a Boundary Layer Model with ShearJournal of the Atmospheric Sciences, 1975
- Three‐dimensional air motion measured in snowGeophysical Research Letters, 1974
- A dual doppler radar method for the determination of wind velocities within precipitating weather systemsRemote Sensing of Environment, 1974
- Stability of stratified shear flowsBoundary-Layer Meteorology, 1973
- Perturbations of Plane Couette Flow in Stratified Fluid and Origin of Cloud StreetsPhysics of Fluids, 1963
- The stability of a shear layer in an unbounded heterogeneous inviscid fluidJournal of Fluid Mechanics, 1958
- Effect of variation in density on the stability of superposed streams of FluidProceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character, 1931